GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of Geology Exclusive of North America, Geological Society of America, Boulder, CO, United States

Abstract

In the area between Loch Katrine and Loch Venachar in the southern Scottish Highlands, the Ben Ledi grits occur as part of the Dalradian graywackes. In a northwestern belt the grits show strongly folded fracture cleavage, and in a southeastern belt unfolded fracture cleavage. The implications are discussed, and resemblance to a similar relation of structures in the Moine schists of Morar is noted.